Multifractal Analysis of Element Distribution in Skarn-type Deposits in the Shizishan Orefield, Tongling Area, Anhui Province, China   总被引：3，自引：1，他引：2  

Wang Qingfei  Deng Jun  Wan Li  Zhao Jie  Gong Qingjie  Yang Liqiang  Zhou Lei  Zhang Zhijun 《《地质学报》英文版》2008,82(4):896-905

A series of element concentrations sampled from four drill cores with a length about 1000 m into different skarn-type deposits were selected from the Shizishan orefield, central Tongling, southeastern part of Anhui Province. Using the multifractal method, the distribution and migration characteristics of the major and trace elements are analyzed. The multifractal spectrum of the major elements is left-skewed, whereas the spectrum of the trace elements is right-skewed, which shows that in the process of skarn formation, the trace elements were enriched only locally, and major elements transported within a much larger range. The correlation coefficients of the multifractal parameters Aa （width of the multifractal spectrum） of the four drill cores are relatively low, but the correlation coefficients of the multifractal parameters R （spectrum symmetry parameter） and Af are relatively higher, indicating that although the non-homogeneous intensity of the distribution of elements is inconsistent, their spatial accumulation patterns are almost the same during the ore-forming process. The statistics of the mnltifractal parameters of various elements in the different locations show that the ore-forming processes and element migration pattern in the Shizishan orefield are consistent, and that the migrations of trace elements and major elements exhibit some differences.  相似文献   

底部弱层非规则布置隔震结构的计算研究   总被引：1，自引：0，他引：1  

李向真  王铁成  雷丽 《世界地震工程》2006,22(4):84-88

提出了层单元方法,将楼板视为剪切弯曲深梁,用二次位移函数和一次转角函数描述楼面运动。同时建立了平面非规则房屋隔震结构动力反应的计算模型,用反应谱方法和时程分析方法计算分析了U型和L型底部弱层非规则布置隔震结构的局部变形的基本动力性能。  相似文献   

天然气水合物资源量估算方法及应用     

梁金强  吴能友  杨木壮  王明君  沙志彬 《地质通报》2006,(Z2)

近年大量的勘探与研究成果表明,中国南海海域具有良好的水合物资源前景。根据所掌握的勘探资料,尝试利用“概率统计法”对南海海域水合物资源前景进行了初步预测,在50%概率的条件下,南海海域的水合物资源量约为649.68×1011m3,与众多学者对全球天然气水合物资源量的估算相似。由于目前勘探程度较低和很多评价参数不能准确给定,因此对南海海域天然气水合物资源量的估算是初步的。该项研究旨在探索天然气水合物资源量的评估方法,随着勘探、研究程度的深入和评价资料的增多,水合物资源量的评价精度将会得到进一步的提高。  相似文献   

典型构造蚀变岩型金矿远景资源量数学模型与预测   总被引：2，自引：0，他引：2  

王庆飞  万丽  刘学飞 《矿床地质》2007,26(3):341-345

数学模型是矿床深部资源量定量化预测一个重要手段,其中品位-吨位模型是一个广泛应用的数学模型,在该模型中,远景资源量为研究区源岩中成矿元素总量的函数。利用该模型,计算胶东构造蚀变岩型金矿远景资源量时,发现由于成矿源岩范围难以确定,而使模型应用准确性受到制约。基于断裂带蚀变岩型金矿的特征,修正了品位-吨位模型。在修正后的模型中,远景资源量为蚀变岩总质量的函数,另包括3个参数:蚀变区元素背景含量(由多标度分形决定)、元素工业品位及矿体品位分布分维值。利用修正后的品位-吨位模型,有效地估算了胶东大尹格庄金矿-1000m以上的理想金属量,得出远景矿石量为5.26×107t,金属量为2.89×105kg,与实际地质情况相吻合。  相似文献   

Mkn501长期光变性质     

杨江河  樊军辉  刘怡  王永祥  杨如曙 《天文学报》2007,48(4):407-417

在R和I波段对Mkn 501进行了测光观测,并结合历史文献得到Mkn 501在近30年间的光学、红外和射电等多个波段的光变曲线;讨论了光变与色指数之间的关系,发现色指数(B—V)与(B—R)之间有强相关,相关系数r=0.73.利用DCF方法分析了多波段光变的相关性,发现B波段与4.8GHz和红外波段的光变存在一定的正相关,利用CLEANest方法对B波段的光变曲线进行频谱分析,结果表明Mkn 501的光变曲线存在2个可能的周期,即(10.06±0.04)年和(21.60±0.17)年.  相似文献   

基于加速器控制网的GPS绝对测量精度探讨     

马娜  董岚  梁静  向伟  罗涛  王铜  刘璨  柯志勇  何振强 《北京测绘》2014,(6):23-27

针对当前散裂中子源准直测量控制网空间距离大、绝对精度要求高,常规测量难以满足需要的问题,提出采用不受通视限制、高精度的GPS测量解决,通过GPS在“标准检测场”准直实验,计算分析后处理软件、观测仪器及观测时长对GPS绝对测量精度的影响,结果表明,1km的测区范围,商业软件解算结果优于科研软件,且商业软件中TTC解算精度最高;分体机比一体机观测精度更高,但随观测时长增长,二者精度相当;观测时长超过8小时以上,基线值将趋于稳定。  相似文献   

基于Theil指数的广东省入境旅游经济时空差异研究     

王建军 《地域研究与开发》2012,31(1):99-103,115

运用Theil指数定量评价了1990-2009年广东省入境旅游经济时空尺度上的市际、地带间和地带内差异变化状况,其结论如下:(1)在时间尺度上,广东入境旅游经济市际差异Tp、地带内差异Twr演变呈逐渐收敛趋同的阶梯状下降趋势;珠三角地带间及地带内差异也呈阶梯状下降,东翼、西翼、山区地带间及地带内演变趋势不明显.(2)在空间尺度上,广东省入境旅游经济发展存在非均衡性,市际差异Tp主要来源于地带内差异Twr的贡献,尤其是珠三角地带内差异的贡献;珠三角与东翼、西翼、山区地带间差异较大,而东翼、西翼、山区地带间差异很小,地带间差异Tbr指数珠三角＞东翼＞山区＞西翼.引入区域分离Separation(缩写为SEP)指数来定量比较广东省四大地带入境旅游经济分离收敛的空间变化规律,并对广东省入境旅游经济发展提出相关建议.  相似文献   

考虑液-固耦合的大型超高压换流变压器地震响应研究          下载免费PDF全文

陈传新  刘彦辉  贺瑞  陈寅  谭平 《地震工程学报》2017,39(3):397-403

针对大型超高压换流变压器的地震响应问题,以一超高压±800kV换流变压器为研究对象,考虑其本体中油与箱壁的相互作用建立三维有限元分析模型,采用LS-DYNA分析换流变压器的自振特性、地震作用下的动力响应规律以及换流变压器的薄弱部位。研究结果显示,对于大型超高压换流变压器,本体中油与箱壁的相互作用对结构动力响应有一定的放大作用,进行自振特性和地震响应分析时应考虑;套管体系的薄弱部位为套管的底部和中间部位,在这两个位置拉应力和压应力最大值交替出现;换流变套管体系在地震作用下的位移较大,套管顶部的导线应设置足够大的伸缩距离。  相似文献   

High-precision relocation of the aftershock sequence of the January 8, 2022, MS6.9 Menyuan earthquake          下载免费PDF全文

Liping Fan  Boren Li  Shirong Liao  Ce Jiang  Lihua Fang 《地震科学（英文版）》2022,35(2):138-145

The 2022 Menyuan M_S6.9 earthquake, which occurred on January 8, is the most destructive earthquake to occur near the Lenglongling (LLL) fault since the 2016 Menyuan M_S6.4 earthquake. We relocated the mainshock and aftershocks with phase arrival time observations for three days after the mainshock from the Qinghai Seismic Network using the double-difference method. The total length and width of the aftershock sequence are approximately 32 km and 5 km, respectively, and the aftershocks are mainly concentrated at a depth of 7–12 km. The relocated sequence can be divided into 18 km west and 13 km east segments with a boundary approximately 5 km east of the mainshock, where aftershocks are sparse. The east and west fault structures revealed by aftershock locations differ significantly. The west fault strikes EW and inclines to the south at a 71º–90º angle, whereas the east fault strikes 133º and has a smaller dip angle. Elastic strain accumulates at conjunctions of faults with different slip rates where it is prone to large earthquakes. Based on surface traces of faults, the distribution of relocated earthquake sequence and surface ruptures, the mainshock was determined to have occurred at the conjunction of the Tuolaishan (TLS) fault and LLL fault, and the west and east segments of the aftershock sequence were on the TLS fault and LLL fault, respectively. Aftershocks migrate in the early and late stages of the earthquake sequence. In the first 1.5 h after the mainshock, aftershocks expand westward from the mainshock. In the late stage, seismicity on the northeast side of the east fault is higher than that in other regions. The migration rate of the west segment of the aftershock sequence is approximately 4.5 km/decade and the afterslip may exist in the source region.  相似文献   

A nearly analytic symplectic partitioned Runge–Kutta method based on a locally one-dimensional technique for solving two-dimensional acoustic wave equations     

Chol Sim  Chunyou Sun  Nam Yun 《Geophysical Prospecting》2020,68(4):1253-1269

In this paper, we develop a new nearly analytic symplectic partitioned Runge–Kutta method based on locally one-dimensional technique for numerically solving two-dimensional acoustic wave equations. We first split two-dimensional acoustic wave equation into the local one-dimensional equations and transform each of the split equations into a Hamiltonian system. Then, we use both a nearly analytic discrete operator and a central difference operator to approximate the high-order spatial differential operators, which implies the symmetry of the discretized spatial differential operators, and we employ the partitioned second-order symplectic Runge–Kutta method to numerically solve the resulted semi-discrete Hamiltonian ordinary differential equations, which results in fully discretized scheme is symplectic unlike conventional nearly analytic symplectic partitioned Runge–Kutta methods. Theoretical analyses show that the nearly analytic symplectic partitioned Runge–Kutta method based on locally one-dimensional technique exhibits great higher stability limits and less numerical dispersion than the nearly analytic symplectic partitioned Runge–Kutta method. Numerical experiments are conducted to verify advantages of the nearly analytic symplectic partitioned Runge–Kutta method based on locally one-dimensional technique, such as their computational efficiency, stability, numerical dispersion and long-term calculation capability.  相似文献